THE DYNAMIC CRUST

What causes earthquakes?
Earthquakes occur when stress builds up in zones of weakness in the earth’s crust. These areas are known as faults. The released energy from a broken fault radiates in all directions. The epicenter is the term used for the point directly over the earthquake on the surface.
Measuring Earthquakes
A Seismologist is a person who studies earthquakes. The scientific tool they use is called a seismograph. During an earthquake, the earth shakes. How much it shakes is called the magnitude.


Earthquake waves
P-waves are also known as primary waves. This is because they travel the fastest.
P-waves are also known as compressional waves which can be thought of as a “push/ pull” movement.
P-waves travel through all materials.
S-waves are also known as secondary waves because they travel slower and ALWAYS arrive after P-waves.
S-waves travel like light waves in that they are “side to side” waves.
S-waves only travel through Solids (S=S).

Locating an epicenter
This has to do with figuring out the difference in P-wave and S-wave arrival times. The closer (in minutes and seconds) they are together, the closer you are to the epicenter. Conversely, the farther the time between P-waves and S-waves, the farther you are located away from the epicenter.


Brain Teaser:
If they occur at the same exact time, where are you located???